“…This vegetation would also have a limited influence on the blowing snow transport, which would already be restricted due to the warmer snow conditions. While there is an ongoing need to improve the understanding and parametrization of individual processes, such as glacier evolution, this focus on individual processes must occur in concert with the understanding of the system and the connections between the processes (Aubry‐Wake, Bertoncini, & Pomeroy, 2022; Aubry‐Wake, Pradhananga, et al., 2022; Drenkhan et al., 2022; Somers et al., 2019). Reducing mountain hydrological changes to only glacier change, as is sometimes done with the peak water concept, might explain why this elusive regime shift is often not discernible in actual mountain streamflow (Stahl et al., 2021; van Tiel, Freudiger, et al., 2021).…”